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Boulder Park National Natural Landmark, of Douglas County, Washington, along with the nearby McNeil Canyon Haystack Rocks and Sims Corner Eskers and Kames natural landmarks, illustrate well-preserved examples of classic Pleistocene ice stagnation landforms that are found in Washington. These landforms include numerous glacial erratics and haystack rocks that occur near and on the Withrow Moraine, which is the terminal moraine of the Okanogan ice lobe.

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  • Boulder Park (en)
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  • Boulder Park National Natural Landmark, of Douglas County, Washington, along with the nearby McNeil Canyon Haystack Rocks and Sims Corner Eskers and Kames natural landmarks, illustrate well-preserved examples of classic Pleistocene ice stagnation landforms that are found in Washington. These landforms include numerous glacial erratics and haystack rocks that occur near and on the Withrow Moraine, which is the terminal moraine of the Okanogan ice lobe. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Glacial-Drift-PB110031.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Erratics-Cascades-PB110028.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Erratics-PB110026.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Terminal-Morraine-PB110030.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Mixed-Eratics-PB110053.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Yeager-Rock-Erractic-PB110039.jpg
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  • 47.87861111111111 -119.80166666666666
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  • Boulder Park National Natural Landmark, of Douglas County, Washington, along with the nearby McNeil Canyon Haystack Rocks and Sims Corner Eskers and Kames natural landmarks, illustrate well-preserved examples of classic Pleistocene ice stagnation landforms that are found in Washington. These landforms include numerous glacial erratics and haystack rocks that occur near and on the Withrow Moraine, which is the terminal moraine of the Okanogan ice lobe. (en)
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