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  • The high mesa in Zion National Park, Utah. Zion National Park is located in the Southwestern United States, near Springdale, Utah. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to half a mile (800 m) deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft (1,117 m) at Coalpits Wash and the highest elevation is 8,726 ft (2,660 m) at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches.
    ZionMesaCreekTreeHorizontal1.jpg
  • Zion National Park
    ZionMesaCreekAfterRain1.jpg
  • Heavy rain quickly floods the streets in Bangkok, Thailand
    BangkokRain1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowCathedral1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsTrees1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0956.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsRocks1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsBend1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0875.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsWide1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    VirginRiverFlow2.jpg
  • Zion National Park is a United States National Park located in southwestern Utah. A prominent feature of the 229-square-mile park is Zion Canyon, which is 15 miles long and up to half a mile deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft  at Coalpits Wash and the highest elevation is 8,726 ft at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches.
    JacksTreeBent1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsCascades1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsRockyStream1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0927.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    VirginRiverFlow2.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0827-HDR-Edit.jpg
  • Zion National Park is a United States National Park located in southwestern Utah. A prominent feature of the 229-square-mile park is Zion Canyon, which is 15 miles long and up to half a mile deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft  at Coalpits Wash and the highest elevation is 8,726 ft at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches.
    JacksTreeBent1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A1048-HDR-Edit.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A1044-HDR.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A1048-HDR-Edit.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A1044-HDR.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowCathedral1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsSlot1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsTwoRocks1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0985-HDR.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsCascades1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsRockyStream1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0951-HDR.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0927.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsFlow1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    VirginRiverNarrows1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0827-HDR-Edit.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsSlot1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsTwoRocks1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0985-HDR.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsTrees1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0956.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0951-HDR.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsRocks1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsFlow1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsBend1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    _Y6A0875.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    NarrowsWide1.jpg
  • The Narrows in Zion National Park, (near Springdale, Utah) is a section of canyon on the North Fork of the Virgin River. The hike of The Narrows is one of the premier hikes on the Colorado Plateau. The term The Narrows refers to both the through-hike of The Narrows, and to The Narrows themselves, especially the 3.6 miles (5.8 km) long section of canyon between the end of the Riverside Walk Trail and Big Spring. The Narrows lies north of, and upstream of, the main Zion Canyon. Hiking the Narrows was rated # 5 in the National Geographic ranking of America's Best 100 Adventures
    VirginRiverNarrows1.jpg
  • The high mesa in Zion National Park, Utah. Zion National Park is located in the Southwestern United States, near Springdale, Utah. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to half a mile (800 m) deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft (1,117 m) at Coalpits Wash and the highest elevation is 8,726 ft (2,660 m) at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches.
    ZionMesaCreekSandstone1.jpg
  • Caprock Canyons State Park and Trailway is a Texas state park on the Caprock Escarpment in Briscoe County, Texas, United States, approximately 100 miles (160 km) southeast of Amarillo. The state park opened in 1982 and is 15,313.6 acres (6,197.2 ha) in size, making it the third-largest state park in Texas.
    CaprockOasis1.jpg
  • Death Valley is a desert valley located in Eastern California. Situated within the Mojave Desert, it is the lowest and driest area in North America. <br />
<br />
Badwater is a salt flat that is beneath the face of the Black Mountains that contains the lowest elevation in North America at 86 meters below sea level. The massive expanse of white is made up of almost pure table salt. This pan was first created by the drying-up of 30-foot deep Recent Lake 2000 to 3000 years ago. Unlike at the Devils Golf Course, significant rainstorms flood Badwater, covering the salt pan with a thin sheet of standing water. Each newly formed lake doesn't last long though, because the 1.9 inch average rainfall is overwhelmed by a 150-inch annual evaporation rate. This, the nation's greatest evaporation potential, means that even a 12-foot deep, 30 mile long lake would dry up in a single year. While flooded, some of the salt is dissolved, then is redeposited as clean, sparkling crystals when the water evaporates.<br />
<br />
Located near the border of California and Nevada, in the Great Basin, east of the Sierra Nevada mountains, Death Valley constitutes much of Death Valley National Park and is the principal feature of the Mojave and Colorado Deserts Biosphere Reserve. It is located mostly in Inyo County, California. It runs from north to south between the Amargosa Range on the east and the Panamint Range on the west; the Sylvania Mountains and the Owlshead Mountains form its northern and southern boundaries, respectively.
    DeathValleyBadwater1.jpg
  • La Villita Historic Arts Village is an art community in downtown San Antonio, Texas, United States. There are art galleries, stores selling souvenirs, gifts, custom jewelry, pottery, and imported Mexican folk art, as well as several restaurants in the district. La Villita connects to the San Antonio River Walk and its outdoor venue, the Arneson River Theatre. It is close to the Alamo, the Henry B. Gonzalez Convention Center, Rivercenter Mall, and HemisFair Park. It is within walking distance of most downtown hotels.<br />
<br />
Located on the south bank of the San Antonio River, La Villita was one of San Antonio's first neighborhoods. In 1939, as ground broke on the San Antonio River Walk development, city officials led by Mayor Maury Maverick acted to preserve this part of San Antonio's history. It was a Native American settlement and then a collection of primitive brush huts, called jacales, for the Spanish soldiers (and their Indian wives and children) stationed nearby at the Mission San Antonio de Valero (an active mission from about 1718 to 1793, now better known as the Alamo). After a flood in 1819 washed away most of the huts, more substantial adobe houses replaced them.
    SanAntonioVillita2.jpg
  • La Villita Historic Arts Village is an art community in downtown San Antonio, Texas, United States. There are art galleries, stores selling souvenirs, gifts, custom jewelry, pottery, and imported Mexican folk art, as well as several restaurants in the district. La Villita connects to the San Antonio River Walk and its outdoor venue, the Arneson River Theatre. It is close to the Alamo, the Henry B. Gonzalez Convention Center, Rivercenter Mall, and HemisFair Park. It is within walking distance of most downtown hotels.<br />
<br />
Located on the south bank of the San Antonio River, La Villita was one of San Antonio's first neighborhoods. In 1939, as ground broke on the San Antonio River Walk development, city officials led by Mayor Maury Maverick acted to preserve this part of San Antonio's history. It was a Native American settlement and then a collection of primitive brush huts, called jacales, for the Spanish soldiers (and their Indian wives and children) stationed nearby at the Mission San Antonio de Valero (an active mission from about 1718 to 1793, now better known as the Alamo). After a flood in 1819 washed away most of the huts, more substantial adobe houses replaced them.
    SanAntonioVillita1.jpg
  • The Chapel of Thanksgiving is a small, spiral tower that features an enclave for prayerful thanks. The entrance to the chapel is at the end of a 125-foot (38 m) bridge that runs over a cascading waterfall. Inside the chapel, the spiral is topped with stained glass windows, leaving a flood of color when looking up in the chapel. Collectively, the stained glass, which was designed by Gabriel Loire of Chartres, France is called the Glory Window. It was designed to feature brighter colors as the spiral reached its apex, becoming brighter and brighter as it reached the center.
    DallasThanksgivingChapel2.jpg
  • The Chapel of Thanksgiving is a small, spiral tower that features an enclave for prayerful thanks. The entrance to the chapel is at the end of a 125-foot (38 m) bridge that runs over a cascading waterfall. Inside the chapel, the spiral is topped with stained glass windows, leaving a flood of color when looking up in the chapel. Collectively, the stained glass, which was designed by Gabriel Loire of Chartres, France is called the Glory Window. It was designed to feature brighter colors as the spiral reached its apex, becoming brighter and brighter as it reached the center.
    StainedGlassSpiral2.jpg
  • The river Arno and Ponte Vecchio bridge in Firenze (Florence), Italy.<br />
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Captured with a Canon 5D Mk III camera and Canon EF 24-105/4L IS lens  <br />
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Florence (Italian: Firenze) is the capital city of the Italian region of Tuscany and of the province of Florence. The Ponte Vecchio ("Old Bridge") is a Medieval stone closed-spandrel segmental arch bridge over the Arno River, in Florence, Italy, noted for still having shops built along it, as was once common. Butchers initially occupied the shops; the present tenants are jewellers, art dealers and souvenir sellers. The Ponte Vecchio's two neighbouring bridges are the Ponte Santa Trinita and the Ponte alle Grazie. The bridge spans the Arno at its narrowest point where it is believed that a bridge was first built in Roman times, when the via Cassia crossed the river at this point. The Roman piers were of stone, the superstructure of wood. The bridge first appears in a document of 996. After being destroyed by a flood in 1117 it was reconstructed in stone but swept away again in 1333 save two of its central piers, as noted by Giovanni Villani in his Nuova Cronica. It was rebuilt in 1345, Giorgio Vasari recorded the tradition in his day, that attributed its design to Taddeo Gaddi, besides Giotto one of the few artistic names of the trecento still recalled two hundred years later. Modern historians present Neri di Fioravanti as a possible candidate. Sheltered in a little loggia at the central opening of the bridge is a weathered dedication stone, which once read Nel trentatrè dopo il mille-trecento, il ponte cadde, per diluvio dell' acque: poi dieci anni, come al Comun piacque, rifatto fu con questo adornamento. The Torre dei Mannelli was built at the southeast corner of the bridge to defend it.<br />
The bridge consists of three segmental arches: the main arch has a span of 30 meters (98 ft) the two side arches each span 27 meters (88 ft). The rise of the arches is between 3.5 and 4.4 meters (11½ to 14½ feet), and the spa
    Ponte Vecchio1.jpg
  • The Chapel of Thanksgiving is a small, spiral tower that features an enclave for prayerful thanks. The entrance to the chapel is at the end of a 125-foot (38 m) bridge that runs over a cascading waterfall. Inside the chapel, the spiral is topped with stained glass windows, leaving a flood of color when looking up in the chapel. Collectively, the stained glass, which was designed by Gabriel Loire of Chartres, France is called the Glory Window. It was designed to feature brighter colors as the spiral reached its apex, becoming brighter and brighter as it reached the center.
    StainedGlassSpiral3.jpg
  • The Chapel of Thanksgiving is a small, spiral tower that features an enclave for prayerful thanks. The entrance to the chapel is at the end of a 125-foot (38 m) bridge that runs over a cascading waterfall. Inside the chapel, the spiral is topped with stained glass windows, leaving a flood of color when looking up in the chapel. Collectively, the stained glass, which was designed by Gabriel Loire of Chartres, France is called the Glory Window. It was designed to feature brighter colors as the spiral reached its apex, becoming brighter and brighter as it reached the center.
    StainedGlassSpiral2.jpg
  • The Chapel of Thanksgiving is a small, spiral tower that features an enclave for prayerful thanks. The entrance to the chapel is at the end of a 125-foot (38 m) bridge that runs over a cascading waterfall. Inside the chapel, the spiral is topped with stained glass windows, leaving a flood of color when looking up in the chapel. Collectively, the stained glass, which was designed by Gabriel Loire of Chartres, France is called the Glory Window. It was designed to feature brighter colors as the spiral reached its apex, becoming brighter and brighter as it reached the center.
    DallasThanksgivingChapel2.jpg
  • The Chapel of Thanksgiving is a small, spiral tower that features an enclave for prayerful thanks. The entrance to the chapel is at the end of a 125-foot (38 m) bridge that runs over a cascading waterfall. Inside the chapel, the spiral is topped with stained glass windows, leaving a flood of color when looking up in the chapel. Collectively, the stained glass, which was designed by Gabriel Loire of Chartres, France is called the Glory Window. It was designed to feature brighter colors as the spiral reached its apex, becoming brighter and brighter as it reached the center.
    DallasThanksgivingChapel1.jpg
  • The Chapel of Thanksgiving is a small, spiral tower that features an enclave for prayerful thanks. The entrance to the chapel is at the end of a 125-foot (38 m) bridge that runs over a cascading waterfall. Inside the chapel, the spiral is topped with stained glass windows, leaving a flood of color when looking up in the chapel. Collectively, the stained glass, which was designed by Gabriel Loire of Chartres, France is called the Glory Window. It was designed to feature brighter colors as the spiral reached its apex, becoming brighter and brighter as it reached the center.
    StainedGlassSpiral3.jpg
  • The Chapel of Thanksgiving is a small, spiral tower that features an enclave for prayerful thanks. The entrance to the chapel is at the end of a 125-foot (38 m) bridge that runs over a cascading waterfall. Inside the chapel, the spiral is topped with stained glass windows, leaving a flood of color when looking up in the chapel. Collectively, the stained glass, which was designed by Gabriel Loire of Chartres, France is called the Glory Window. It was designed to feature brighter colors as the spiral reached its apex, becoming brighter and brighter as it reached the center.
    StainedGlassSpiral1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityFence3.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei7.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei4.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei3.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei2.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop5.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    BluebonnetCow1.jpg
  • Navajo Bridge crosses the Colorado River's Marble Canyon near Lee's Ferry in the US state of Arizona. Apart from the Glen Canyon Bridge a few miles upstream at Page, Arizona, it is the only roadway crossing of the river and the Grand Canyon for nearly 600 miles (970 km). Spanning Marble Canyon, the bridge carries northbound travelers to southern Utah and to the Arizona Strip, the otherwise inaccessible portion of Arizona north of the Colorado River, which includes the North Rim of Grand Canyon National Park.<br />
Prior to the construction of the first Navajo Bridge, the only river crossing from Arizona to Utah was at nearby Lee's Ferry, where the canyon walls are low and getting vehicles onto the water is relatively convenient. The ferry offered only unreliable service, however, as adverse weather and flooding regularly prevented its operation.
    NavajoBridge1.jpg
  • Navajo Bridge crosses the Colorado River's Marble Canyon near Lee's Ferry in the US state of Arizona. Apart from the Glen Canyon Bridge a few miles upstream at Page, Arizona, it is the only roadway crossing of the river and the Grand Canyon for nearly 600 miles (970 km). Spanning Marble Canyon, the bridge carries northbound travelers to southern Utah and to the Arizona Strip, the otherwise inaccessible portion of Arizona north of the Colorado River, which includes the North Rim of Grand Canyon National Park.<br />
Prior to the construction of the first Navajo Bridge, the only river crossing from Arizona to Utah was at nearby Lee's Ferry, where the canyon walls are low and getting vehicles onto the water is relatively convenient. The ferry offered only unreliable service, however, as adverse weather and flooding regularly prevented its operation.
    NavajoBridge1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop6.jpg
  • Galveston is a coastal city located on Galveston Island and Pelican Island in the U.S. state of Texas. Named after Bernardo de Gálvez y Madrid, Count of Gálvez (born in Málaga, Spain), Galveston's first European settlements on the island were constructed around 1816 by French pirate Louis-Michel Aury to help the fledgling Republic of Mexico fight Spain. The Port of Galveston was established in 1825 by the Congress of Mexico following its successful independence from Spain. The city served as the main port for the Texas Navy during the Texas Revolution, and later served as the capital of the Republic of Texas. During the 19th century, Galveston became a major U.S. commercial center and one of the largest ports in the United States. It was devastated by the 1900 Galveston Hurricane, whose effects included flooding and a storm surge. The natural disaster on the exposed barrier island is still ranked as the deadliest in United States history, with an estimated toll of 8,000 people.
    PleasurePier1.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei15.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei9.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei8.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei6.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei5.jpg
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
<br />
In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
<br />
The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop12.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityRoad2.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop4.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop3.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    WillowCityLoop1.jpg
  • The Texas Hill Country is a twenty-five county region of Central Texas and South Texas featuring karst topography and tall rugged hills consisting of thin layers of soil atop limestone or granite. It also includes the Llano Uplift and the second largest granite dome in the United States, Enchanted Rock. The Hill Country reaches into portions of the two major metropolitan areas, especially in San Antonio's northern suburbs and the western half of Travis County, ending southwest of Downtown Austin. The region is the eastern portion of the Edwards Plateau and is bound by the Balcones Fault on the east and the Llano Uplift to the west and north. The terrain is punctuated by a large number of limestone or granite rocks and boulders and a thin layer of topsoil, which makes the region very dry and prone to flash flooding. The Texas Hill Country is also home to several native types of vegetation, such as various yucca, prickly pear cactus, cedar scrub, and the dry Southwestern tree known as the Texas live oak.
    AtascosaField1.jpg
  • Pampas deer (Ozotoceros bezoarticus) live in the grasslands of South America at low elevations. They are known as venado or gama in Spanish and as veado-campeiro in Portuguese. Their habitat includes water and hills, often with winter drought, and grass that is high enough to cover a standing deer. Many of them live on the Pantanal wetlands, where there are ongoing conservation efforts, and other areas of annual flooding cycles. Human activity has changed much of the original landscape. They are known to live up to 12 years in the wild, longer if captive, but are threatened due to over-hunting and habitat loss. Many people are concerned over this loss, because a healthy deer population means a healthy grassland, and a healthy grassland is home to many species, some also threatened. Many North American birds migrate south to these areas, and if the Pampas deer habitat is lost, they are afraid these bird species will also decline. There are approximately 80,000 Pampas deer total, with the majority of them living in Brazil.
    _D3_5137.jpg
  • Pampas deer (Ozotoceros bezoarticus) live in the grasslands of South America at low elevations. They are known as venado or gama in Spanish and as veado-campeiro in Portuguese. Their habitat includes water and hills, often with winter drought, and grass that is high enough to cover a standing deer. Many of them live on the Pantanal wetlands, where there are ongoing conservation efforts, and other areas of annual flooding cycles. Human activity has changed much of the original landscape. They are known to live up to 12 years in the wild, longer if captive, but are threatened due to over-hunting and habitat loss. Many people are concerned over this loss, because a healthy deer population means a healthy grassland, and a healthy grassland is home to many species, some also threatened. Many North American birds migrate south to these areas, and if the Pampas deer habitat is lost, they are afraid these bird species will also decline. There are approximately 80,000 Pampas deer total, with the majority of them living in Brazil.
    PampasDeer1.jpg
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