Sunday 6 December 2009

Motoring in the Mojave Desert – 19th to 23rd November 2009

Directly south of Death Valley is one the newest units in the National Park system; the Mojave National Preserve is an area of the Mojave desert with very little development in it.

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In the north are the remains of Volcanic cinder cones and lava flows, The area has numerous fault lines and in geological terms these are fairly new.

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Near the cinder cones were “Mojave Joshua Trees” which were neither trees or Cactus but a type of Yucca and a member of the lily family yet growing to well over 20 ft tall.

 

 

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Then after 30 miles or so there is a 3 track railway, and a station building which houses one of the Park visitor centres. 60 years ago this was a busy mining area supplying steel to build ships for the US navy.

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We continued to the Hole in the Wall campground, which was next to a strange looking rock formation formed by a steam and magma explosion when the cloud of material solidified rapidly.

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The explosion lasted about half a second and solid “cloud” extends  about a quarter mile long and 200ft high.

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With the aid of steel rings in the rocks we climbed up through Banshee Canyon.

 

 

We were amazed at the number of plants growing in the desert.

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IMG_3344 Out of the Mojave NP we travelled a short section of “Old Route 66” to the Amboy Crater, meeting a couple who were adding their own memento to the shoe tree.

 

 

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Last active only 500 years ago the Amboy crater is accessible and we were able to climb into crater where I went to the rim edge 200ft above the surrounding desert and lava flow remains.

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Elaine in the crater bottom.

Discovering Death Valley – 16th to 19th November 2009

Scorchingly hot in July and August when temperatures reach 49 deg C, the valley was pleasantly warm (25-30 deg C) in November. IMG_2967 IMG_3000 IMG_3009 

 

Colourful mountains and canyons

to explore,

 

 

 

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sand dunes to walk over

 

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Salt flats at the lowest land location in America

 

 

 

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where the little water that exists contains 5 times more salt than sea water and most is below a deep, dry and crisp crust,

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and industrial relics of Borax mills which struggled to remain viable in the late 1800’s.

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