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The Big Lava Bed, located in the Gifford Pinchot National Forest in the southwestern area of the State of Washington, originated from a 500-foot-deep crater in the northern center of the bed. The Big Lava Bed is the youngest feature of the Indian Heaven volcanic field. The 0.9-cubic kilometer lava flow erupted from the cinder cone about 8200 years ago. The lava flow traveled 13 km from the source crater. Lodgepole pine, alder, and other pioneer plants struggle to grow, seen sparsely growing between and amid towering rock piles, caves, and strange lava formations. Access into the interior of the lava bed is difficult, since there are no roads or trails crossing the lava field. Explorers who wish to venture deep within the lava flow are advised to choose their route carefully. Compasses are

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  • Big Lava Bed (en)
  • Big Lava Bed (de)
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  • The Big Lava Bed, located in the Gifford Pinchot National Forest in the southwestern area of the State of Washington, originated from a 500-foot-deep crater in the northern center of the bed. The Big Lava Bed is the youngest feature of the Indian Heaven volcanic field. The 0.9-cubic kilometer lava flow erupted from the cinder cone about 8200 years ago. The lava flow traveled 13 km from the source crater. Lodgepole pine, alder, and other pioneer plants struggle to grow, seen sparsely growing between and amid towering rock piles, caves, and strange lava formations. Access into the interior of the lava bed is difficult, since there are no roads or trails crossing the lava field. Explorers who wish to venture deep within the lava flow are advised to choose their route carefully. Compasses are (en)
  • Das Big Lava Bed ist ein Lavafeld im Gifford Pinchot National Forest, liegt im Südwesten des US-Bundesstaates Washington und entstammt einem 500 ft (152 m) tiefen Vulkankrater im nördlichen Zentrum des Lavafeldes. Das Big Lava Bed ist das jüngste Objekt im Vulkanfeld Indian Heaven. Der Lavafluss von 0,9 Kubikkilometern Volumen wurde von einem Schlackenkegel vor etwa 8.200 Jahren ausgestoßen. Der Lavastrom floss über 13 Kilometer von seinem Ursprungsort. Küsten-Kiefern, Erlen und andere Pionierpflanzen begannen zu wachsen und bildeten lichte Bestände inmitten von hohen Felssäulen, Höhlen und bizarren Lavastrukturen. Der Zugang ins Innere des Lavafeldes ist schwierig, weil keine Straßen und Wege zu ihm hin oder darüber hinweg führen. Entdecker sind angehalten, ihre Routen sorgfältig zu wähle (de)
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  • Big Lava Bed (en)
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  • Big Lava Bed (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Big_Lava_Bed.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Indian_Heaven_Volcanic_Field_Satellite_Map.png
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