Death Valley For New Year's Eve, 2009-2010
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You'll need to shake the sand out of your shoes after checking this out. Come with Lisa and I as we usher in the new decade by experiencing towering sand dunes, strange castles in the middle of nowhere, otherworldly landscapes, fiery red sunsets, and haunted hotels with a one-person opera show still going for over 40 years. Come with us as we explore Death Valley. |
![]() Gettin' our Kix on Route 66. Yeah. |
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![]() Death Valley Junction grew from a tent town to a borax mining town in the early 1900s. Now, it's a desert ghost town, population three.
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![]() The Opera House and the hotel were constructed in the 1920s by the Pacific Borax Mining company, who built the town to accommodate its mine workers. An uninhabited area of the hotel is said to contain hauntings. Guests and workers have reported phantom smells, to the sounds of babies crying to full bodied apparitions. Lisa and I heard murmurings during the night, but alas, these were simply people walking past. We felt cold spots, but really, the entire hotel was cold. The next morning, I took a tour of the Opera House with Amber, the supervisor for the Amargosa Hotel. |
![]() She bought the place, went to NY to collect her belongings, moved to Death Valley Junction, and has never been back to NY since. She singlehandedly restored the Opera House for her solo performances, further repairing and painting it after a flash flood. Attracting audiences to a ghost town miles into the harsh desert is no easy feat. When Marta first began, she'd perform for audiences of one. Undaunted, she simply painted an audience on the wall. Amber said that Marta was now 85, and had recently broken a hip and had stopped performing for the moment. I found her story and achievements inspiring, and would love to see her perform. Let's hope she does. |
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![]() The highs? Death Valley holds the record for the highest (reliably reported) temperature in the Western Hemisphere, 134°F (56.7°C). The lows? Badwater Basin in Death Valley has the lowest elevation in North America, 282 ft (85.5m) below sea level. Lisa had been sick, but the moisture-starved desert air healed her up in no time, ironic for a place called Death Valley.
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![]() How did this happen? It's a fascinating combination of large blocks of bedrock sinkiing and seismic activity shoving the surrounding Panamint and Amargosa Mountains up good and high. And for added interest, add intense heat and volcanic activity, and you have Death Valley. The shimmering white expanse of Badwater Basin.
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![]() Death Valley wasn't always dry. 2000 to 4000 years ago, streams from the nearby mountains filled Death Valley with 30 feet of water. However, the climate warmed and the rain virtually stopped, drying up the water, and leaving concentrated minerals and salty pools. The salts crystallized into a thick 3-5 ft. crust on the basin floor, with billions of crunchy salt crystals. Another look at the crystallized salt floor of Badwater Basin.
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Death Valley, California 2009-2010
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Contact photographer/musician Ken Lee