Friday, June 13, 2014

Day 8 Las Vegas to Mammoth Lakes – 315 miles

We left the Luxor hotel fairly early and headed to the Las Vegas Eaglerider depot to meet up with people who were in the second team on last week’s tour leg and also new joiners for the second part of the tour.  


After some delay we set off back into the scrub desert north west of Las Vegas, stopping for petrol at the unusually named town of Pahrump. Crossing over the California state line we headed into Death Valley – somewhat apprehensively given that today’s date was Friday the 13th.  We stopped for a team photo at the park boundary and then continued to Zabriske viewpoint.






At Furnace Creek – some 200 feet below sea level - we halted for water before steeling ourselves to ride without stopping through the rest of Death Valley given the sweltering heat.  We passed the Devil’s Cornfield and the Sand Dunes and gained a few thousand feet of altitude before stopping for a break near Darwin Falls.

Above image from the web
Above image from the web






In various places the Death Valley scenery resembled ‘Mordor’ whilst turning westwards we could see the Sierra Nevada – still with remnants of snow – and more reminiscent of the ‘Misty Mountains’.



We stopped at Lone Pine for a late-ish lunch.  The hills near Lone Pine have been the location for numerous western film sequences and the restaurant walls were festooned with photos and posters of stars in their prime.


Lone Pine

We rode northwards along a high level, wide valley with volcanic outcrops but increasingly lush vegetation as a consequence of streams from the Sierra Nevada.  At Bishop we rested by an idyllic stream complete with ducks – more English than US.









After a final 50 mile stretch we arrived at Mammoth Lakes.  The temperature was lower than we had anticipated so we quickly retired to our rooms before exploring the local restaurants.

Music Links:






Comedy Video:



Death Valley Background:
Death Valley is the lowest and driest area in North America with Badwater Basin  at 282 feet (86 m) below sea level.
The depth and shape of Death Valley influence its summer temperatures being walled by high, steep mountain ranges. The clear, dry air and sparse plant cover allow sunlight to heat the desert surface.
During the ice age which ended roughly 10,000–12,000 years ago, the Sierra Nevada was much wetter. During that time, Death Valley was filled with a huge lake that was nearly 100 miles long and 600 feet deep.
Death Valley is home to the Timbisha tribe of Native Americans, formerly known as the Panamint Shoshone, who have inhabited the valley for at least the past millennium. The Timbisha name for the valley, tümpisa, means "rock paint" and refers to the red ochre paint that can be made from a type of clay found in the valley.
The valley received its English name in 1849 during the California Gold Rush. It was called Death Valley by prospectors and others who sought to cross the valley on their way to the gold fields, although only one death in the area was recorded during the Rush. During the 1850s, gold and silver were extracted in the valley. In the 1880s, borax was discovered and extracted by mule-drawn wagons.

Death Valley National Monument was proclaimed on February 11, 1933, by President Herbert Hoover, placing the area under federal protection. In 1994, the monument was redesignated as Death Valley National Park, as well as being substantially expanded to include Saline and Eureka Valleys.

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