Brand: vendor-unknown

Color Of Canvas:

  • Full Color
  • Sepia
  • Black and White

Size Of Canvas:

  • 18X24
  • 27X36
  • 36X54
  • 3-10x20
  • 3-12x24
  • 3-16x32
  • 3-20x40
  • 3-24x48
  • 3-30x60

Type Of Canvas:

  • Rolled Canvas ( no frame )
  • Triptych Canvas

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Product Description

Looking Out the Front Door Orem UT Canvas Prints

Mount Timpanogos, sometimes informally referred to as Timp, is the second highest mountain in Utah's Wasatch Range. Timpanogos rises to an elevation of 11,752 ft (3,582 m) above sea level in the Uinta-Wasatch-Cache National Forest. With 5,270 feet of topographic prominence, Timpanogos is the 47th-most prominent mountain in the contiguous United States.The mountain towers over Utah Valley, including the cities of Lehi, Provo, Orem, Pleasant Grove, American Fork, Lindon and others. The exposed portion of the mountain is made up entirely of limestone and dolomite from the Pennsylvanian period, and is about 300 million years old. Heavy winter snowfall is characteristic of this portion of the Wasatch Range, and avalanche activity is common in winter and spring. The mountain is also home to Timpanogos Cave National Monument, a series of decorated caves in the north end of the mountain that have guided ranger tours open daily to the public during the warmer months. The word Timpanogos comes from the Timpanogots tribe who lived in the surrounding valleys from AD 1400. The name translates as "rock" (tumpi-), and "water mouth" or "canyon" (panogos).Mount Timpanogos displays many examples of various glacial processes and the sculpting power of moving ice. Ice Age glaciers mantled the peak until relatively recently, and dramatically shaped the mountain into an Alpine tableau of knife-edge ridges and yawning, U-shaped amphitheaters. A remnant of these glaciers persists in the deeply recessed hanging valley below the main summit. Timpanogos Glacier is a rock-covered mass found on a long, north-facing slope, and usually has patches of snow the entire year. Although an above ground cirque glacier was present before the Dust Bowl Drought of the 1930s, no glacial ice is visible today. However, in 1994, a large crevasse opened up, revealing that there still is a glacier buried beneath the talus.

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