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  • From Männlichen Gipfel see the peaks of Eiger (Ogre 13,026 feet on left), Mönch (Monk), and Jungfrau (Virgin 13,600 feet on right) in the Berner Oberland, Switzerland, the Alps, Europe. Grindelwald Valley drops left and Lauterbrunnen Valley right. The world's longest continuous rack and pinion railway (Wengernalpbahn) goes from Grindelwald up to Kleine Scheidegg and down to Wengen and Lauterbrunnen. From Kleine Scheidegg, another cog train (Jungfraubahn) ascends steeply inside the Eiger to Jungfraujoch, the highest railway station in Europe. A gondola (gondelbahn) connects Grindelwald with Männlichen, where a cable car goes down to Wengen (Luftseilbahn Wengen-Männlichen). From Männlichen station, walk uphill 15 minutes for a stunning summit view. Published on the cover of Ryder Walker Alpine Adventures 2005 Catalog. Published in September/October 2004 Sierra Magazine (Sierra Club Outings, double page opening spread). Published in Wilderness Travel 2000, 1993, 2014 Catalog of Adventures, and 2015 Private Journeys. Featured in a Swiss movie by Meret Nora Burger.
    81ALP-04-15_Eiger-Monch-Jungfrau_MAS...jpg
  • Hikers walk a dog along a rock face near Northgate Peaks trail, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1053.jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 10 overlapping photos.
    1303UT-1139-1148pan_Zion-NP_Kolob-Te...jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 8 overlapping photos.
    1303UT-1122-1129pan_Zion-NP_Kolob-Te...jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1134-p1.jpg
  • Deer cross Kolob Terrace Road at entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1118.jpg
  • Deer cross Kolob Terrace Road at entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1103.jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1070.jpg
  • View from Kolob Terrace Road towards peaks of Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1057.jpg
  • A hiker rests at the end of Northgate Peaks trail, in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 5 overlapping photos.
    1303UT-1031-35pan_Zion_Northgate-Pea...jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1157.jpg
  • Deer cross Kolob Terrace Road at entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1105.jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1121.jpg
  • La Virgen de Quito, on Panecillo hill, is an aluminum statue of the winged virgin (45 meters tall), inspired and enlarged from Bernardo de Lagarda's 1734 sculpture on display on the main altar in San Francisco Church, Quito, Ecuador, South America. This madonna was created in 1976 by Spanish artist Agustín de la Herrán Matorras. The virgin stands on top of a globe and is stepping on a snake. The wings are unusual in the tradition of madonna icons. Seen to the south of downtown Quito, the Panecillo hill looks like a “small bread roll” (its Spanish translation) and stands at about 3000m (9840 feet). Before the Spanish arrived, the Incas worship the sun on Shungoloma, or Hill of the Heart (present-day Panecillo).  Later, from 1812 to 1815, the Spanish constructed a fortress on the hill to control people below. Visit from Old Town via inexpensive taxi. See panoramic 360° views of Quito from here, best early in the morning (around 10:00 am), before the clouds form on nearby mountains. On a clear day, see Cotopaxi in the distance.  UNESCO honored City of Quito as a World Heritage Site in 1978. Quito was founded in 1534 on the ruins of an Inca city. Despite the 1917 earthquake, the city has the best-preserved, least altered historic center in Latin America.
    94GAL-02-05_Virgin-of-Panecillo_Quit...jpg
  • The sandstone cliffs of the Court of the Patriarchs tower over the Virgin River in Zion National Park, near Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. (Panorama stitched from 6 photos.)
    11UT1-2001-06pan_Zion-NP-Utah.jpg
  • A foot bridge crosses the Virgin River in Zion National Park, near Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. (Panorama stitched from 6 photos.)
    11UT1-2237-42pan_Zion-NP-Utah.jpg
  • The sandstone cliffs of the Court of the Patriarchs tower over the Virgin River in Zion National Park, near Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2014_Zion-NP-Utah.jpg
  • The sandstone cliffs of the Court of the Patriarchs tower over the Virgin River in Zion National Park, near Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. (Panorama stitched from 6 photos.)
    11UT1-2007-12pan_Zion-NP-Utah.jpg
  • The peaks of Eiger, Mönch, and Jungfrau (Ogre, Monk, and Virgin) reflect in a pond at Kleine Scheidegg in the Berner Oberland, Switzerland, the Alps, Europe. The world's longest continuous rack and pinion railway (Wengernalpbahn) goes from Grindelwald up to Kleine Scheidegg and down to Wengen and Lauterbrunnen. From Kleine Scheidegg, another cog train (Jungfraubahn) ascends steeply inside the Eiger to Jungfraujoch, the highest railway station in Europe. UNESCO lists “Swiss Alps Jungfrau-Aletsch” as a World Heritage Area (2001, 2007). Panorama stitched from six images. Published in September/October 2007 Sierra Magazine, Sierra Club Outings. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    05ALP_0056-61pan_Eiger-Monch-Jungfra...jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2164_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2030_Zion-NP-Utah.jpg
  • Good Friday, April 10, 2009 in Quito, Ecuador, Pichincha province, South America: The Virgen Dolorosa (Virgin of Sorrows) is paraded in Quito’s great procession of Good Friday, which starts and ends at the San Francisco church and passes through Quito’s historic center. Good Friday was the day when Jesus Christ was sentenced and crucified.
    09ECU-1264_Quito-Ecuador.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2238_Zion-NP-Utah-p2.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2236_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2221_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2215-18pan_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2092-2101pan_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2173-77pan_Zion-NP-Utah.jpg
  • This colorful old Greek Orthodox Christian fresco ceiling is at Sumela Monastery, under restoration in this 1999 image. The 1000-year-old Monastery of the Virgin Mary at Sumela is among the most impressive sights of Turkey's Black Sea coast. The monastery, founded in AD 386, clings to a cliff above a cool evergreen forest in Altindere National Park, in the Maçka district of Trabzon Province in the modern Republic of Turkey. The Sumela Monastery (Greek: Μονή Παναγίας Σουμελά, Moní Panagías Soumelá; Turkish: Sümela Manastırı) is a Greek Orthodox monastery dedicated to the Virgin Mary (Panagia, meaning "All Holy" in Greek) at Melá Mountain (Turkish: KaradaÄŸ, which is a direct translation of the Greek name Ssou Melá, "Black Mountain") within the Pontic Mountains (Turkish: Kuzey Anadolu DaÄŸları) range.
    99TUR-37-12mod_Sumela-Monastery-fres...jpg
  • Holy Assumption of the Virgin Mary Russian Orthodox Church was built in 1896 in Kenai, Alaska, USA. It is a  National Historic Landmark, and the oldest standing Orthodox church in Alaska.
    06AK_1033_Russian-Church-1896_Kenai.jpg
  • In a large painting in St Giles' Cathedral, a Scottish unicorn paired with an English lion defines the coat of arms of James VI, as the first king of Great Britain and Ireland. What's with the unicorn? Unicorns were first depicted in 2600 BC in ancient seals of the Indus Valley Civilization and were mentioned by the ancient Greeks. In Celtic mythology the unicorn symbolized purity, innocence, masculinity and power. The proud, haughty unicorn was chosen as Scotland's national animal because it would rather die than be captured, just as Scots would fight to remain sovereign and unconquered. The unicorn was first used on the Scottish royal coat of arms by William I in the 1100s, and two unicorns supported the shield until 1603. When James VI became James I of England and Ireland in 1603, he replaced one unicorn with the national animal of England, the lion, to demonstrate unity. Believed to be the strongest of all animals, wild and untamed, the mythical unicorn could only be humbled by a virgin maiden. However, Scotland's unicorn in the coat of arms is always bounded by a golden chain, often shown around its neck and body, symbolizing the power of the Scottish kings, strong enough to tame a unicorn. Today, the version of the royal coat of arms used in Scotland emphasizes Scottish elements, placing the unicorn on the left and giving it a crown, whereas the version used in England and elsewhere places the unicorn on the right and gives English elements more prominence. The Scottish version uses the motto "Nemo me impune lacessit," meaning "No one wounds (touches) me with impunity." The English version says "Dieu et mon droit," meaning "God and my right," the motto of the Monarch of the United Kingdom. St Giles' Cathedral (High Kirk of Edinburgh) is the principal place of worship of the Church of Scotland in Edinburgh.
    17SC1-4401_Scotland.jpg
  • In a large painting in St Giles' Cathedral, a Scottish unicorn paired with an English lion defines the coat of arms of James VI, as the first king of Great Britain and Ireland. What's with the unicorn? Unicorns were first depicted in 2600 BC in ancient seals of the Indus Valley Civilization and were mentioned by the ancient Greeks. In Celtic mythology the unicorn symbolized purity, innocence, masculinity and power. The proud, haughty unicorn was chosen as Scotland's national animal because it would rather die than be captured, just as Scots would fight to remain sovereign and unconquered. The unicorn was first used on the Scottish royal coat of arms by William I in the 1100s, and two unicorns supported the shield until 1603. When James VI became James I of England and Ireland in 1603, he replaced one unicorn with the national animal of England, the lion, to demonstrate unity. Believed to be the strongest of all animals, wild and untamed, the mythical unicorn could only be humbled by a virgin maiden. However, Scotland's unicorn in the coat of arms is always bounded by a golden chain, often shown around its neck and body, symbolizing the power of the Scottish kings, strong enough to tame a unicorn. Today, the version of the royal coat of arms used in Scotland emphasizes Scottish elements, placing the unicorn on the left and giving it a crown, whereas the version used in England and elsewhere places the unicorn on the right and gives English elements more prominence. The Scottish version uses the motto "Nemo me impune lacessit," meaning "No one wounds (touches) me with impunity." The English version says "Dieu et mon droit," meaning "God and my right," the motto of the Monarch of the United Kingdom. St Giles' Cathedral (High Kirk of Edinburgh) is the principal place of worship of the Church of Scotland in Edinburgh.
    17SC1-4398_Scotland.jpg
  • Cliff near Upper Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1215.jpg
  • A water trough at Chuebodmi (in Lauterbrunnen municipality) reflects Mönch (Monk) and Jungfrau (Virgin, 13,600 feet) in the Berner Oberland, Switzerland, the Alps, Europe. The Bernese Highlands are the upper part of Bern Canton. UNESCO lists “Swiss Alps Jungfrau-Aletsch” as a World Heritage Area (2001, 2007).
    05ALP_0142-trough-Monch-Jungfrau.jpg
  • Named for a renegade who hid here in the 1890s, Mouse's Tank is a natural rock basin which holds life-sustaining water for months in the arid desert. In Valley of Fire State Park, walk here for a half-mile round trip on the Petroglyph Canyon Trail. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4082_Valley-of-Fire-SP-Nevada.jpg
  • The Desert Primrose (or Dune Evening Primrose, Oenothera deltoides) flower blooms white with yellow center, opening in the early evening and closing in mid-morning. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4073_Valley-of-Fire-SP-Nevada.jpg
  • Holes erode in sandstone formations on the Petroglyph Canyon Trail, Valley of Fire State Park, Nevada, USA. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1638_Valley-of-Fire-SP-Nevada.jpg
  • Prehistoric native Americans chipped images into the desert varnish on Petroglyph Canyon Trail, Valley of Fire State Park, Nevada, USA. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1635_Valley-of-Fire-SP-Nevada.jpg
  • Prehistoric native Americans chipped images into the desert varnish on Petroglyph Canyon Trail, Valley of Fire State Park, Nevada, USA. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1612_Valley-of-Fire-SP-Nevada.jpg
  • The "Fire Wave" is a one mile round trip walk in the White Domes area of Valley of Fire State Park, the oldest state park in Nevada (dedicated in 1935). Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1578_Valley-of-Fire-SP-Nevada-...jpg
  • The "Fire Wave" is a one mile round trip walk in the White Domes area of Valley of Fire State Park, the oldest state park in Nevada (dedicated in 1935). Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation. (Panorama stitched from 12 photos.)
    11NV1-1530-41pan_Valley-of-Fire-SP-N...jpg
  • The "Fire Wave" is a one mile round trip walk in the White Domes area of Valley of Fire State Park, the oldest state park in Nevada (dedicated in 1935). Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1521-23pan_Valley-of-Fire-SP-N...jpg
  • Sunset light illuminates colorful orange, pink, yellow, and white sandstone in White Domes area of Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1486_Valley-of-Fire-SP-Nevada.jpg
  • Sunset light illuminates colorful orange, pink, yellow, and white sandstone in White Domes area of Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1466_Valley-of-Fire-SP-Nevada.jpg
  • Conglomerate rocks lie on red and white striped sandstone in White Domes area of Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1446_Valley-of-Fire-SP-Nevada.jpg
  • Sunset light illuminates colorful orange, pink, yellow, and white sandstone in White Domes area of Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1396_Valley-of-Fire-SP-Nevada.jpg
  • The White Domes trail passes through a slot canyon striped with orange and white sandstone in Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1314_Valley-of-Fire-SP-Nevada.jpg
  • The "Fire Wave" is a one mile round trip walk in the White Domes area of Valley of Fire State Park, the oldest state park in Nevada (dedicated in 1935). Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1129_Valley-of-Fire-SP-Nevada.jpg
  • The "Fire Wave" is a one mile round trip walk in the White Domes area of Valley of Fire State Park, the oldest state park in Nevada (dedicated in 1935). Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1087_Valley-of-Fire-SP-Nevada.jpg
  • Native Americans created the petroglyphs at Atlatl Rock over 4000 years ago. The art reflects their thoughts, but we can only guess at their meaning. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1031_Valley-of-Fire-SP-Nevada.jpg
  • Arch Rock Campground. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1018_Valley-of-Fire-SP-Nevada.jpg
  • Hikers ascend impressive switchbacks of the West Rim Trail on the way to Angels Landing and Scout Lookout. Zion National Park adjoins Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2220_Zion-NP-Utah.jpg
  • Snow coats a tree in a mossy canyon in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2055_Zion-NP-Utah.jpg
  • Snow coats a tree in a mossy canyon in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2052_Zion-NP-Utah.jpg
  • Morning sun backlights a cottonwood tree in Zion National Park, which adjoins Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2022_Zion-NP-Utah.jpg
  • A local islander pumps a foot-powered loom to weave the famous Harris Tweed at Gearrannan Blackhouse Village on the Isle of Lewis, Outer Hebrides (Western Isles), Scotland, United Kingdom, Europe. The Orb Trademark, pressed onto every length of cloth and seen on the traditional woven label affixed to finished items, guarantees the highest quality, 100% pure new wool Harris Tweed, dyed, spun and handwoven by islanders of the Outer Hebrides of Scotland at their homes, to the laws enshrined in the 1993 Harris Tweed Act of Parliament. First woven in the 1700s by crafters in the Outer Hebrides, Harris Tweed was introduced to the British aristocracy in the 1840s by Lady Dunmore. To regulate and protect the fabric against imitations, the Harris Tweed Orb certification mark was created in 1909 (the oldest British mark of its kind). Today, the yarn is no longer hand spun, a change introduced with the Hattersley mark 1 loom, the first operated by feet. Most of the required virgin wool is now sourced from mainland Scotland. Harris Tweed is truly "dyed in the wool," that is, dyed prior to being spun. Gearrannan Blackhouse Village features 9 restored traditional thatched cottages, built in the late 1800s and lived in until 1974, the last to be inhabited in the Western Isles. This image was stitched from 2 overlapping photos.
    17SC1-31333-34-Pano_Scotland.jpg
  • In a large painting in St Giles' Cathedral, a Scottish unicorn paired with an English lion defines the coat of arms of James VI, as the first king of Great Britain and Ireland. What's with the unicorn? Unicorns were first depicted in 2600 BC in ancient seals of the Indus Valley Civilization and were mentioned by the ancient Greeks. In Celtic mythology the unicorn symbolized purity, innocence, masculinity and power. The proud, haughty unicorn was chosen as Scotland's national animal because it would rather die than be captured, just as Scots would fight to remain sovereign and unconquered. The unicorn was first used on the Scottish royal coat of arms by William I in the 1100s, and two unicorns supported the shield until 1603. When James VI became James I of England and Ireland in 1603, he replaced one unicorn with the national animal of England, the lion, to demonstrate unity. Believed to be the strongest of all animals, wild and untamed, the mythical unicorn could only be humbled by a virgin maiden. However, Scotland's unicorn in the coat of arms is always bounded by a golden chain, often shown around its neck and body, symbolizing the power of the Scottish kings, strong enough to tame a unicorn. Today, the version of the royal coat of arms used in Scotland emphasizes Scottish elements, placing the unicorn on the left and giving it a crown, whereas the version used in England and elsewhere places the unicorn on the right and gives English elements more prominence. The Scottish version uses the motto "Nemo me impune lacessit," meaning "No one wounds (touches) me with impunity." The English version says "Dieu et mon droit," meaning "God and my right," the motto of the Monarch of the United Kingdom. St Giles' Cathedral (High Kirk of Edinburgh) is the principal place of worship of the Church of Scotland in Edinburgh.
    17SC1-4400_Scotland.jpg
  • Inside Stirling Castle, unicorns in the Scottish King's Bedchamber symbolize royal purity & strength. What's with the unicorn? Unicorns were first depicted in 2600 BC in ancient seals of the Indus Valley Civilization and were mentioned by the ancient Greeks. In Celtic mythology the unicorn symbolized purity, innocence, masculinity and power. The proud, haughty unicorn was chosen as Scotland's national animal because it would rather die than be captured, just as Scots would fight to remain sovereign and unconquered. The unicorn was first used on the Scottish royal coat of arms by William I in the 1100s, and two unicorns supported the shield until 1603. When James VI became James I of England and Ireland in 1603, he replaced one unicorn with the national animal of England, the lion, to demonstrate unity. Believed to be the strongest of all animals, wild and untamed, the mythical unicorn could only be humbled by a virgin maiden. However, Scotland's unicorn in the coat of arms is always bounded by a golden chain, often shown around its neck and body, symbolizing the power of the Scottish kings, strong enough to tame a unicorn. Most of Stirling Castle's main buildings date from the 1400s and 1500s, when it peaked in importance. Scotland, United Kingdom, Europe. This image was stitched from several overlapping photos.
    17SC1-2096-2100-Pano_Scotland.jpg
  • In Bram Stoker's famous 1897 novel, Dracula came ashore as a creature resembling a large dog who climbed the dramatic 199 Church Steps to the graveyard of Church of Saint Mary, shown here atop East Cliff, above Whitby at the mouth of the Esk River. The Church of Saint Mary the Virgin is an Anglican parish church serving the towns of Whitby and Ruswarp in North Yorkshire county, England, United Kingdom, Europe. Founded around 1110 AD, the church has a tower and transepts dating from the 1100s and 1200s, and interior dating mostly from the late 1700s. Seen on our England Coast to Coast hike day 13 of 14. [This image, commissioned by Wilderness Travel, is not available to any other agency providing group travel in the UK, but may otherwise be licensable from Tom Dempsey – please inquire at PhotoSeek.com.] This image was stitched from multiple overlapping photos.
    17UK-6769-75pan.jpg
  • The Church Steps above Whitby: In Bram Stoker's famous 1897 novel, Dracula came ashore as a creature resembling a large dog who climbed the dramatic 199 Church Steps to the graveyard of Church of Saint Mary, adjacent to Whitby Abbey ruins atop East Cliff, above the Esk River. The Church of Saint Mary the Virgin is an Anglican parish church serving the towns of Whitby and Ruswarp in North Yorkshire county, England, United Kingdom, Europe. England Coast to Coast hike day 13 of 14. [This image, commissioned by Wilderness Travel, is not available to any other agency providing group travel in the UK, but may otherwise be licensable from Tom Dempsey – please inquire at PhotoSeek.com.] This image was stitched from multiple overlapping photos.
    17UK-6789-91pan.jpg
  • Whitby at the mouth of the Esk River, seen from Dracula's Church Steps, in England, United Kingdom, Europe. In Bram Stoker's famous 1897 novel, Dracula came ashore as a creature resembling a large dog who climbed the dramatic 199 Church Steps to the graveyard of Church of Saint Mary, adjacent to Whitby Abbey ruins atop East Cliff, above the Esk River. The Church of Saint Mary the Virgin is an Anglican parish church serving the towns of Whitby and Ruswarp in North Yorkshire county. This was at the end of our England Coast to Coast hike, on day 13 of 14. The next day, our 14th, ended being dropped off in York. [This image, commissioned by Wilderness Travel, is not available to any other agency providing group travel in the UK, but may otherwise be licensable from Tom Dempsey – please inquire at PhotoSeek.com.]
    17UK-6800_England.jpg
  • The Anglican "Parish Church of Saint Mary the Virgin" dates from the 1100s-1200s, with major restoration in 1860, on the Holy Island of Lindisfarne, Northumberland, England, United Kingdom, Europe. Holy Island history dates from the 500s AD as an important center of Celtic Christianity under Saints Aidan of Lindisfarne, Cuthbert, Eadfrith of Lindisfarne, and Eadberht of Lindisfarne. After Viking invasions and the Norman conquest of England, a priory was reestablished. A small castle was built on Holy Island in 1550.
    17UK2-5107.jpg
  • Statue of the Roman goddess Diana at Allerton Garden, on the south shore of Kauai, Hawaii, USA. In Roman mythology, Diana was the goddess of the hunt, the moon, and nature (associated with wild animals, woodland, and talking to and controlling animals), and virgin goddess of childbirth and women. She was one of the three maiden goddesses, along with Minerva and Vesta, who swore never to marry. Although she was eventually conflated with the Greek goddess Artemis, she arose independentently in Italy. Deer and oak groves were especially sacred to her. According to mythology (in common with the Greek religion and their deity Artemis), Diana was born with her twin brother, Apollo, on the island of Delos, daughter of Jupiter and Latona. Nestled in a valley transected by the Lawai Stream ending in Lawai Bay, Allerton Garden is one of five gardens of the non-profit National Tropical Botanical Garden (ntbg.org). Address: 4425 Lawai Rd, Koloa, HI 96756.
    1701HAW-1970.jpg
  • Statue of the Roman goddess Diana at Allerton Garden, on the south shore of Kauai, Hawaii, USA. In Roman mythology, Diana was the goddess of the hunt, the moon, and nature (associated with wild animals, woodland, and talking to and controlling animals), and virgin goddess of childbirth and women. She was one of the three maiden goddesses, along with Minerva and Vesta, who swore never to marry. Although she was eventually conflated with the Greek goddess Artemis, she arose independentently in Italy. Deer and oak groves were especially sacred to her. According to mythology (in common with the Greek religion and their deity Artemis), Diana was born with her twin brother, Apollo, on the island of Delos, daughter of Jupiter and Latona. Nestled in a valley transected by the Lawai Stream ending in Lawai Bay, Allerton Garden is one of five gardens of the non-profit National Tropical Botanical Garden (ntbg.org). Address: 4425 Lawai Rd, Koloa, HI 96756.
    1701HAW-1968.jpg
  • Statue of the Roman goddess Diana at Allerton Garden, on the south shore of Kauai, Hawaii, USA. In Roman mythology, Diana was the goddess of the hunt, the moon, and nature (associated with wild animals, woodland, and talking to and controlling animals), and virgin goddess of childbirth and women. She was one of the three maiden goddesses, along with Minerva and Vesta, who swore never to marry. Although she was eventually conflated with the Greek goddess Artemis, she arose independentently in Italy. Deer and oak groves were especially sacred to her. According to mythology (in common with the Greek religion and their deity Artemis), Diana was born with her twin brother, Apollo, on the island of Delos, daughter of Jupiter and Latona. Nestled in a valley transected by the Lawai Stream ending in Lawai Bay, Allerton Garden is one of five gardens of the non-profit National Tropical Botanical Garden (ntbg.org). Address: 4425 Lawai Rd, Koloa, HI 96756.
    1701HAW-1965.jpg
  • Walk the trail behind Lower Emerald Pool waterfall in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 5 overlapping photos.
    1303UT-1236-1240pan_Lower-Emerald-Fa...jpg
  • Upper Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 7 overlapping photos.
    1303UT-1220-1226PAN_Upper-Emerald-Po...jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1212.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1209.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1205.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1196.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1186.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1191.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1184.jpg
  • Patterns of desert varnish coat canyon walls near Lower Emerald Pool waterfall in Zion National Park, Springdale, Utah, USA. Manganese-rich desert varnish requires thousands of years to coat a rock face that is protected from precipitation and wind erosion. The varnish likely originates from airborne dust and external surface runoff, including: clay minerals, oxides and hydroxides of manganese (Mn) and/or iron (Fe), sand grains, trace elements, and usually organic matter. Streaks of black varnish often occur where water cascades over cliffs, but wind doesn't sculpt its shape. Varnish color varies from shades of brown to black. Manganese-poor, iron-rich varnishes are red to orange, and intermediate concentrations are shaded brown. Manganese-oxidizing microbes may explain the unusually high concentration of manganese in black desert varnish, which can be smooth and shiny where densest. More about Zion: The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UTC-5012.jpg
  • In the National Archaeological Museum in Athens, Greece, see a Roman model of the "Athena Polias" ("Athena of the city") sculpture which was placed in the Parthenon in 432 BC, originally 12 meters high. Athena (Athene or Athina) has Nike in her right hand, and sphinx and griffins in her headpiece. Greeks built the Parthenon atop the Acropolis in 447-438 BCE as a place to worship goddess Athena and also as a treasury to store tribute money moved from Delos Island. The Greek philosopher, Plato (429347 BC), identified Athena with the Libyan deity Neith who was the war goddess and huntress deity of the Egyptians since the ancient Pre-Dynastic period, and who was also identified with weaving. Athena is the virgin patron of her namesake city Athens, and is goddess of wisdom, courage, inspiration, civilization, law and justice, just warfare, mathematics, strength, strategy, the arts, crafts, and skill. Minerva, Athena's Roman incarnation, embodies similar attributes.
    01GRE-29-13_Roman-model-of-Athina-Po...jpg
  • The Metropolitan Cathedral of Quito (La Catedral Metropolitana; or officially: Catedral Primada de la Virgen Asunta al Cielo Primatial, which means Cathedral of the Assumption of Our Lady to Heaven) is located in Independence Plaza, Quito, Ecuador, South America. The official church was built by 1565, with additions and renovations completed by 1806. The arches feature late Gothic design; the main altar is more Baroque in nature; the choir area is Neoclassic; and the ceilings boast Moorish styling. The interior includes various artworks such as the “Ascension of the Virgin” by Manuel Samaniego; a piece by Caspicara entitled “Descent of Christ from the Cross”; and paintings created at the School of Quito. The Metropolitan Cathedral of Quito contains the tomb of Mariscal Sucre, Antonio Jose de Sucre, Cardinal de la Torre and some of the Republic's presidents as well as other priests and bishops. Cardinal de la Torre was born Carlos Maria Javier in Quito on 14 November 1873. He became the first Roman Catholic bishop in Ecuador to be promoted to cardinal. He died in 1968 and was buried at the cathedral. UNESCO honored City of Quito as a World Heritage Site in 1978. Quito was founded in 1534 on the ruins of an Inca city. Despite the 1917 earthquake, the city has the best-preserved, least altered historic center in Latin America.
    09ECU-1257_Quito-Ecuador.jpg
  • The Metropolitan Cathedral of Quito (La Catedral Metropolitana; or officially: Catedral Primada de la Virgen Asunta al Cielo Primatial, which means Cathedral of the Assumption of Our Lady to Heaven) is located in Independence Plaza, Quito, Ecuador, South America. The official church was built by 1565, with additions and renovations completed by 1806. The arches feature late Gothic design; the main altar is more Baroque in nature; the choir area is Neoclassic; and the ceilings boast Moorish styling. The interior includes various artworks such as the “Ascension of the Virgin” by Manuel Samaniego; a piece by Caspicara entitled “Descent of Christ from the Cross”; and paintings created at the School of Quito. The Metropolitan Cathedral of Quito contains the tomb of Mariscal Sucre, Antonio Jose de Sucre, Cardinal de la Torre and some of the Republic's presidents as well as other priests and bishops. Cardinal de la Torre was born Carlos Maria Javier in Quito on 14 November 1873. He became the first Roman Catholic bishop in Ecuador to be promoted to cardinal. He died in 1968 and was buried at the cathedral. UNESCO honored City of Quito as a World Heritage Site in 1978. Quito was founded in 1534 on the ruins of an Inca city. Despite the 1917 earthquake, the city has the best-preserved, least altered historic center in Latin America.
    09ECU-1256_Quito-Ecuador.jpg
  • Thousands of people participate in Quito’s great procession of Good Friday, which was the day when Jesus Christ was sentenced and crucified. Captured April 10, 2009 in Quito, Ecuador, Pichincha province, South America. The hooded cucuruchos and the robed Verónicas are the traditional figures who accompany Jesús del Gran Poder (Jesus Almighty) and the Virgen Dolorosa (Virgin of Sorrows) on the procession which starts and ends at the San Francisco church and passes through Quito’s historic center. The cucuruchos symbolize the penitents who, dressed in purple, show their repentance and their will to change. (The traditional conical, pointed-hat robes resemble those worn in Spain and famously by the Klu-Klux Klan; Cucurucho is Spanish for cone or cornet.) Many penitents carry crosses, chain their feet, or wrap thorns around their heads. The Verónicas recall the woman who came to Jesus as he carried the cross, and who wiped his face full of sweat and blood. In Quito, the Verónicas also wear purple, their faces hidden by black shrouds.
    09ECU-1249_Quito-Ecuador.jpg
  • From Männlichen, see Jungfrau ("The Virgin" 4158 meters or 13,642 feet elevation) and Lauterbrunnen Valley in the Berner Oberland, Switzerland, the Alps, Europe. UNESCO lists “Swiss Alps Jungfrau-Aletsch” as a World Heritage Area (2001, 2007). The Bernese Highlands are the upper part of Bern Canton, Switzerland. Published in Wilderness Travel Catalog of Adventures 1995, 1991.
    81ALP-04-22_Jungfrau-Mannlichen.jpg
  • From Wasenegg Ridge, see mountain peaks of Eiger (the Ogre, 13,026 feet), Mönch (the Monk), Jungfrau (the Virgin, 13,600 feet), and Lauterbrunnen Wall in the Berner Oberland, Switzerland, the Alps, Europe. The Bernese Highlands are the upper part of Bern Canton. Panorama stitched from 3 overlapping photos. UNESCO lists “Swiss Alps Jungfrau-Aletsch” as a World Heritage Area (2001, 2007).
    05ALP_0309-311pan-Lauterbrunnen-Wall.jpg
  • Three women hike Wasenegg Ridge. Left to right are Eiger (the Ogre, 13,026 feet), Mönch (the Monk), and Jungfrau (the Virgin, 13,600 feet) in the Berner Oberland, Switzerland, the Alps, Europe. The Bernese Highlands are the upper part of Bern Canton. UNESCO lists “Swiss Alps Jungfrau-Aletsch” as a World Heritage Area (2001, 2007). Published in Wilderness Travel 2017 Catalog of Adventures.
    05ALP_0243-Wasenegg-hikers-Eiger-Mon...jpg
  • Wavy sandstone pattern by Carol Dempsey, Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    99NV-C2-13-wavy-sandstone_Valley-of-...jpg
  • Banded pink and yellow sandstone in Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    99NV-03-37_pink-yellow-sandstone_Val...jpg
  • Banded pink and yellow sandstone in Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    99NV-03-19_pink-sandstone_Valley-of-...jpg
  • Mammatus clouds bulge beneath cumulonimbus clouds over yellow and red sandstone on the White Domes trail in Valley of Fire State Park,  Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    95NV-15-15_Valley-of-Fire-SP.jpg
  • A barrel cactus grows on red and white sandstone in White Domes area of Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV3C-5127.jpg
  • Red, yellow, and white sandstone erodes into fascinating shapes in the White Domes area in Valley of Fire State Park, Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV3C-5117.jpg
  • The Desert Primrose (or Dune Evening Primrose, Oenothera deltoides) flower blooms white with yellow center, opening in the early evening and closing in mid-morning. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV3C-5028.jpg
  • The Desert Primrose (or Dune Evening Primrose, Oenothera deltoides) flower blooms white with yellow center, opening in the early evening and closing in mid-morning. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4075_Valley-of-Fire-SP-Nevada.jpg
  • Desert Primrose (or Dune Evening Primrose,<br />
Oenothera deltoides) flowers bloom white with yellow center, opening in the early evening and closing in mid-morning. Valley of Fire State Park (dedicated in 1935) is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park’s fiery red sandstone formations. The park also has fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610–790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4074_Valley-of-Fire-SP-Nevada.jpg
  • Cholla cactus grows sharp yellow spines amid white and red sandstone formations in White Domes area of Valley of Fire State Park (dedicated in 1935) in Nevada, USA. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4058_Valley-of-Fire-SP-Nevada.jpg
  • The Desert Primrose (or Dune Evening Primrose, Oenothera deltoides) flower blooms white with yellow center, opening in the early evening and closing in mid-morning. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4051_Valley-of-Fire-SP-Nevada.jpg
  • The Desert Primrose (or Dune Evening Primrose, Oenothera deltoides) flower blooms white with yellow center, opening in the early evening and closing in mid-morning. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4027_Valley-of-Fire-SP-Nevada.jpg
  • The Desert Primrose (or Dune Evening Primrose, Oenothera deltoides) flower blooms white with yellow center, opening in the early evening and closing in mid-morning. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4021_Valley-of-Fire-SP-Nevada.jpg
  • The Desert Primrose (or Dune Evening Primrose, Oenothera deltoides) flower blooms white with yellow center, opening in the early evening and closing in mid-morning. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park also boasts fascinating patterns in limestone, shale, and conglomerate rock. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV2-4005_Valley-of-Fire-SP-Nevada.jpg
  • Sandstone formations erode and grow lichen on the Petroglyph Canyon Trail, Valley of Fire State Park, Nevada, USA. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1640_Valley-of-Fire-SP-Nevada.jpg
  • Holes erode in sandstone formations on the Petroglyph Canyon Trail, Valley of Fire State Park, Nevada, USA. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1637_Valley-of-Fire-SP-Nevada.jpg
  • Prehistoric native Americans chipped images into the desert varnish on Petroglyph Canyon Trail, Valley of Fire State Park, Nevada, USA. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1615_Valley-of-Fire-SP-Nevada.jpg
  • Sandstone erodes into a snail-like formation in Petroglyph Canyon Trail, Valley of Fire State Park, Nevada, USA. Valley of Fire State Park, dedicated in 1935, is the oldest state park in Nevada. Starting more than 150 million years ago, great shifting sand dunes during the age of dinosaurs were compressed, uplifting, faulted, and eroded to form the park's fiery red sandstone formations. The park adjoins Lake Mead National Recreation Area at the Virgin River confluence, at an elevation of 2000 to 2600 feet (610-790 m), 50 miles (80 km) northeast of Las Vegas, USA. Park entry from Interstate 15 passes through the Moapa Indian Reservation.
    11NV1-1607_Valley-of-Fire-SP-Nevada.jpg
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